ГЕОГРАФИЧЕСКИЙ АНАЛИЗ РАЗВИТИЯ ВЕРТИКАЛЬНЫХ РУСЛОВЫХ ДЕФОРМАЦИЙ НА РЕКАХ ВОСТОЧНОЙ ЕВРОПЫ И АЗИИ

dc.contributor.authorЧалов Р.С.
dc.contributor.authorЛю Шугуан
dc.date.accessioned2024-03-09T07:07:16Z
dc.date.available2024-03-09T07:07:16Z
dc.date.issued2006
dc.description.abstractSpatial regularities of long-term deep erosion and accumulation on the rivers of the East Europe and Asia are analyzed. In the intracontinental regions incision is predominant, its value depending on the velocity of the tectonic uplift. Accumulation appears on the rivers, which cross marginal and littoral lowlands, with its velocity increasing southwards up to enormous values according to the solid runoff growth and the velocity of river mouth prograding. Muddying is characteristic of little rivers of the steppe and south forest zones due to excess of soil erosion material.
dc.identifierhttps://elibrary.ru/item.asp?id=9213553
dc.identifier.citationГеоморфология, 2006, , 1, 86-92
dc.identifier.issn0435-4281
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/42927
dc.subject.udc551.4.435.13(282.247+282.25)
dc.titleГЕОГРАФИЧЕСКИЙ АНАЛИЗ РАЗВИТИЯ ВЕРТИКАЛЬНЫХ РУСЛОВЫХ ДЕФОРМАЦИЙ НА РЕКАХ ВОСТОЧНОЙ ЕВРОПЫ И АЗИИ
dc.typeСтатья

Файлы

Коллекции